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生态系统工程师的形态特征和分类单元身份塑造了真光层-中层过渡带的生物多样性。

Ecosystem engineer morphological traits and taxon identity shape biodiversity across the euphotic-mesophotic transition.

机构信息

Lyell Centre for Earth and Marine Science and Technology, Edinburgh, UK.

School of Energy, Geoscience, Infrastructure and Society, Heriot-Watt University, Edinburgh, UK.

出版信息

Proc Biol Sci. 2022 Feb 23;289(1969):20211834. doi: 10.1098/rspb.2021.1834.

Abstract

The euphotic-mesophotic transition is characterized by dramatic changes in environmental conditions, which can significantly alter the functioning of ecosystem engineers and the structure of their associated communities. However, the drivers of biodiversity change across the euphotic-mesophotic transition remain unclear. Here, we investigated the mechanisms affecting the biodiversity-supporting potential of free-living red coralline algae-globally important habitat creators-towards mesophotic depths. Across a 73 m depth gradient, we observed a general decline in macrofaunal biodiversity (fauna abundance, taxon richness and alpha diversity), but an increase in beta-diversity (i.e. variation between assemblages) at the deepest site (86 m depth, where light levels were less than 1% surface irradiance). We identified a gradient in abundance decline rather than distinct ecological shifts, driven by a complex interaction between declining light availability, declining size of the coralline algal host individuals and a changing host taxonomy. However, despite abundance declines, high between-assemblage variability at deeper depths allowed biodiversity-supporting potential to be maintained, highlighting their importance as coastal refugia.

摘要

真光-中层过渡带的特征是环境条件的剧烈变化,这会显著改变生态系统工程师的功能及其相关群落的结构。然而,真光-中层过渡带的生物多样性变化驱动因素仍不清楚。在这里,我们研究了影响自由生活的红色珊瑚藻(全球重要的生境创造者)在中层深度的生物多样性支持潜力的机制。在 73 米的深度梯度上,我们观察到大型动物生物多样性(动物丰度、分类群丰富度和 alpha 多样性)普遍下降,但在最深的站点(86 米深处,光照水平低于地表辐照度的 1%),beta 多样性(即群落之间的变异)增加。我们发现,丰度下降是由光照可用性下降、珊瑚藻宿主个体大小下降和宿主分类学变化之间的复杂相互作用驱动的,而不是明显的生态转变。然而,尽管丰度下降,深层的群落间变异性很高,仍保持了生物多样性支持潜力,突出了它们作为沿海避难所的重要性。

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